Abstract
The small-strain shear modulus (Gmax) is a soil property that has many practical applications. The authors compiled a database of Gmaxmeasurements for 40 normally consolidated to slightly overconsolidated low to high plasticity clays. Using these data, the authors propose a semi-empirical relationship between Gmax, effective stress (σ'v or σ'c), preconsolidation stress (σ'p) and in-situ void ratio (e0) for four ranges of plasticity index (Ip): Ip < 30%, 30% ≤ Ip < 50%, 50% ≤ Ip < 80% and 80% ≤ Ip < 120%. With results from bender element tests on a Gulf of Mexico clay subjected to multiple load-unload consolidation loops, the authors were able to validate the proposed relationships for 30% ≤ Ip < 50% and 50% ≤ Ip < 80%. The proposed relationship for 30% ≤ Ip < 50% and 50% ≤ Ip < 80% captures changes in laboratory Gmaxresulting from variations in effective stress (σ'c), maximum past stress (σ'v,max), and void ratio. The proposed relationships are a simple and efficient tool that can provide independent insight on Gmaxif the stress history of a clay is known, or on stress history if Gmaxis known.
Highlights
The small-strain shear modulus, Gmax, refers to the ratio of shear stress to shear strain at strains < 10-3%
This paper focuses on the Gmax of soft clays
This paper provides a framework that takes into account effective stress, 'c, preconsolidation stress, 'p, void ratio, e0 and plasticity index, Ip
Summary
The small-strain shear modulus, Gmax, refers to the ratio of shear stress to shear strain at strains < 10-3%. Based on the extensive works done on the Gmax of soft clays, spanning almost 60 years ([8] – [19]), our understanding of the controlling factors has been sharpened These include effective stress, void ratio, plasticity index, preconsolidation stress, anisotropy (inherent and stress-induced), age of deposit, degree of saturation, cementation, thixotropy, and mineralogy. The small-strain shear modulus of a saturated clayey soil is controlled by the stiffness of the matrix, which depends on effective stress, preconsolidation stress, void ratio, stress history, strength anisotropy, plasticity index and mineralogy (among others). The closer the particles, the denser the fabric, the less likely it is to deform in shear, and the larger the stiffness For a clay, both the effective stress and the void ratio control the fabric.
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